工程热物理学报
工程熱物理學報
공정열물이학보
JOURNAL OF ENGINEERING THERMOPHYSICS
2009年
9期
1593-1596
,共4页
林俊光%翁青松%武田直辉%刘银河%刘艳华%车得福
林俊光%翁青鬆%武田直輝%劉銀河%劉豔華%車得福
림준광%옹청송%무전직휘%류은하%류염화%차득복
煤%气化%NO_x%HCN%NH_3
煤%氣化%NO_x%HCN%NH_3
매%기화%NO_x%HCN%NH_3
coal%gasification%NO_x%HCN%NH_3
采用U型管反应系统,研究了氧浓度、气流速率和气化温度对神木煤气化过程中NO_x及其前驱物的释放规律.研究发现:气化时生成的HCN和NH_3总量比热解时大幅下降,表明O_2的引入抑制了H自由基的可获得性.随着氧浓度的增加,NO的收率先减后增,而NO_2收率几乎没有变化.氧浓度较低时,生成的高浓度CO阻止了挥发分氮向NO的转化.气流速率对含氮气相产物释放影响各不相同.低温气化产物以NO_2和HCN为主,NO_2主要来自进样期挥发分的缓慢氧化,而高温气化产物中的NH_3的生成主要来源于焦炭氮.
採用U型管反應繫統,研究瞭氧濃度、氣流速率和氣化溫度對神木煤氣化過程中NO_x及其前驅物的釋放規律.研究髮現:氣化時生成的HCN和NH_3總量比熱解時大幅下降,錶明O_2的引入抑製瞭H自由基的可穫得性.隨著氧濃度的增加,NO的收率先減後增,而NO_2收率幾乎沒有變化.氧濃度較低時,生成的高濃度CO阻止瞭揮髮分氮嚮NO的轉化.氣流速率對含氮氣相產物釋放影響各不相同.低溫氣化產物以NO_2和HCN為主,NO_2主要來自進樣期揮髮分的緩慢氧化,而高溫氣化產物中的NH_3的生成主要來源于焦炭氮.
채용U형관반응계통,연구료양농도、기류속솔화기화온도대신목매기화과정중NO_x급기전구물적석방규률.연구발현:기화시생성적HCN화NH_3총량비열해시대폭하강,표명O_2적인입억제료H자유기적가획득성.수착양농도적증가,NO적수솔선감후증,이NO_2수솔궤호몰유변화.양농도교저시,생성적고농도CO조지료휘발분담향NO적전화.기류속솔대함담기상산물석방영향각불상동.저온기화산물이NO_2화HCN위주,NO_2주요래자진양기휘발분적완만양화,이고온기화산물중적NH_3적생성주요래원우초탄담.
The formation and release of NO_x and its precursors are investigated during the gasification of Shenmu coal in O_2/Ar with a U-type reactor,the effects of oxygen concentration,gas flow rate and gasification temperature are examined.Experimental results show that the yields of HCN and NH_3 during gasification are much less than those during pyrolysis.It suggests that the presence of O_2 inhibit the availability of H radical.The yield of NO first decreases,land then increases with increased oxygen concentration,whereas the yield of NO_2 hardly changes.The high concentration of CO restrains the conversion of volatile-N to NO while oxygen concentration is low.The gas flow rate exerts a different effect on the release of different N-containing gas product.NO_2 and HCN are predominant N-containing products at low temperatures,and NO_2 may originate from the gradual oxidation of volatile-N while NH_3 from char-N at high temperatures.